• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

抛物型方程的时空自适应分层模型约简

Space-time adaptive hierarchical model reduction for parabolic equations.

作者信息

Perotto Simona, Zilio Alessandro

机构信息

MOX, Department of Mathematics, Politecnico di Milano, Piazza Leonardo da Vinci, 32, 20133 Milan, Italy.

Centre d'Analyse et de Mathématique Sociales, École des Hautes Études en Sciences Sociales, 190-198 Avenue de France, 75244 Paris Cedex 13, France.

出版信息

Adv Model Simul Eng Sci. 2015;2:25. doi: 10.1186/s40323-015-0046-4. Epub 2015 Oct 13.

DOI:10.1186/s40323-015-0046-4
PMID:27110492
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC4802829/
Abstract

BACKGROUND

Surrogate solutions and surrogate models for complex problems in many fields of science and engineering represent an important recent research line towards the construction of the best trade-off between modeling reliability and computational efficiency. Among surrogate models, hierarchical model (HiMod) reduction provides an effective approach for phenomena characterized by a dominant direction in their dynamics. HiMod approach obtains 1D models naturally enhanced by the inclusion of the effect of the transverse dynamics.

METHODS

HiMod reduction couples a finite element approximation along the mainstream with a locally tunable modal representation of the transverse dynamics. In particular, we focus on the pointwise HiMod reduction strategy, where the modal tuning is performed on each finite element node. We formalize the pointwise HiMod approach in an unsteady setting, by resorting to a model discontinuous in time, continuous and hierarchically reduced in space (c[M([Formula: see text])G()]-dG() approximation). The selection of the modal distribution and of the space-time discretization is automatically performed via an adaptive procedure based on an analysis of the global error. The final outcome of this procedure is a table, named , that sets the time partition and, for each time interval, the corresponding 1D finite element mesh together with the associated modal distribution.

RESULTS

The results of the numerical verification confirm the robustness of the proposed adaptive procedure in terms of accuracy, sensitivity with respect to the goal quantity and the boundary conditions, and the computational saving. Finally, the validation results in the groundwater experimental setting are promising.

CONCLUSION

The extension of the HiMod reduction to an unsteady framework represents a crucial step with a view to practical engineering applications. Moreover, the results of the validation phase confirm that HiMod approximation is a viable approach.

摘要

背景

在许多科学和工程领域,针对复杂问题的替代解决方案和替代模型是近期一项重要的研究方向,旨在实现建模可靠性和计算效率之间的最佳权衡。在替代模型中,层次模型(HiMod)降阶为具有主导动力学方向的现象提供了一种有效方法。HiMod方法通过纳入横向动力学效应自然地获得一维模型。

方法

HiMod降阶将沿主流方向的有限元近似与横向动力学的局部可调模态表示相结合。具体而言,我们关注逐点HiMod降阶策略,即在每个有限元节点上进行模态调整。我们通过采用一个在时间上不连续、在空间上连续且分层降阶的模型(c[M([公式:见正文])G()]-dG()近似),在非稳态情况下形式化逐点HiMod方法。模态分布和时空离散化的选择通过基于全局误差分析的自适应过程自动进行。该过程的最终结果是一个名为 的表格,它设定了时间划分,并针对每个时间间隔,给出相应的一维有限元网格以及相关的模态分布。

结果

数值验证结果证实了所提出的自适应过程在准确性、对目标量和边界条件的敏感性以及计算节省方面的稳健性。最后,在地下水实验环境中的验证结果很有前景。

结论

将HiMod降阶扩展到非稳态框架是迈向实际工程应用的关键一步。此外,验证阶段的结果证实HiMod近似是一种可行的方法。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/7f4af5c880f6/40323_2015_46_Fig27_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/e15df7485cf3/40323_2015_46_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/9cc45c5f90c3/40323_2015_46_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/ed68784e23bd/40323_2015_46_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/b9c90596b987/40323_2015_46_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/f02f6bfd679e/40323_2015_46_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/e6eb267cd276/40323_2015_46_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/990711c3f86c/40323_2015_46_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/0a8ed376732a/40323_2015_46_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/46e7b7cdd75c/40323_2015_46_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/72674d6fe964/40323_2015_46_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/cab278428613/40323_2015_46_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/9e7a845aa627/40323_2015_46_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/afc64c883ed3/40323_2015_46_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/f9176882250c/40323_2015_46_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/73fcb5c3dbad/40323_2015_46_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/e25e46b08ae3/40323_2015_46_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/2090f0bab554/40323_2015_46_Fig17_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/f42350e01563/40323_2015_46_Fig18_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/465583e6fa29/40323_2015_46_Fig19_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/41b090760594/40323_2015_46_Fig20_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/875515cb123e/40323_2015_46_Fig21_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/ee34cb42dcff/40323_2015_46_Fig22_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/56109fad298e/40323_2015_46_Fig23_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/9795e8a730ae/40323_2015_46_Fig24_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/096fac85e9b0/40323_2015_46_Fig25_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/a106b452011b/40323_2015_46_Fig26_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/7f4af5c880f6/40323_2015_46_Fig27_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/e15df7485cf3/40323_2015_46_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/9cc45c5f90c3/40323_2015_46_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/ed68784e23bd/40323_2015_46_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/b9c90596b987/40323_2015_46_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/f02f6bfd679e/40323_2015_46_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/e6eb267cd276/40323_2015_46_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/990711c3f86c/40323_2015_46_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/0a8ed376732a/40323_2015_46_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/46e7b7cdd75c/40323_2015_46_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/72674d6fe964/40323_2015_46_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/cab278428613/40323_2015_46_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/9e7a845aa627/40323_2015_46_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/afc64c883ed3/40323_2015_46_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/f9176882250c/40323_2015_46_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/73fcb5c3dbad/40323_2015_46_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/e25e46b08ae3/40323_2015_46_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/2090f0bab554/40323_2015_46_Fig17_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/f42350e01563/40323_2015_46_Fig18_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/465583e6fa29/40323_2015_46_Fig19_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/41b090760594/40323_2015_46_Fig20_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/875515cb123e/40323_2015_46_Fig21_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/ee34cb42dcff/40323_2015_46_Fig22_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/56109fad298e/40323_2015_46_Fig23_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/9795e8a730ae/40323_2015_46_Fig24_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/096fac85e9b0/40323_2015_46_Fig25_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/a106b452011b/40323_2015_46_Fig26_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1900/4802829/7f4af5c880f6/40323_2015_46_Fig27_HTML.jpg

相似文献

1
Space-time adaptive hierarchical model reduction for parabolic equations.抛物型方程的时空自适应分层模型约简
Adv Model Simul Eng Sci. 2015;2:25. doi: 10.1186/s40323-015-0046-4. Epub 2015 Oct 13.
2
A numerical study of adaptive space and time discretisations for Gross-Pitaevskii equations.关于格罗斯 - 皮塔耶夫斯基方程的自适应时空离散化的数值研究。
J Comput Phys. 2012 Aug 15;231(20):6665-6681. doi: 10.1016/j.jcp.2012.05.031.
3
A Posteriori Error Estimates for Fully Discrete Finite Element Method for Generalized Diffusion Equation with Delay.具有时滞的广义扩散方程全离散有限元方法的后验误差估计
J Sci Comput. 2020;84(1):13. doi: 10.1007/s10915-020-01262-5. Epub 2020 Jul 1.
4
Space-time adaptive numerical methods for geophysical applications.用于地球物理应用的时空自适应数值方法。
Philos Trans A Math Phys Eng Sci. 2009 Nov 28;367(1907):4613-31. doi: 10.1098/rsta.2009.0158.
5
A posteriori error approximation in discontinuous Galerkin method on polygonal meshes in elliptic problems.椭圆问题中多边形网格上间断 Galerkin 方法的后验误差逼近。
Sci Rep. 2023 Jul 4;13(1):10791. doi: 10.1038/s41598-023-37414-4.
6
Three-dimensional numerical modeling for global cochlear dynamics.用于全球耳蜗动力学的三维数值建模。
J Acoust Soc Am. 2000 Jan;107(1):474-85. doi: 10.1121/1.428352.
7
Space-time finite element methods stabilized using bubble function spaces.使用气泡函数空间稳定化的时空有限元方法。
Appl Anal. 2018 Sep 24;99(7):1153-1170. doi: 10.1080/00036811.2018.1522630. eCollection 2020.
8
Finite element methods for the biomechanics of soft hydrated tissues: nonlinear analysis and adaptive control of meshes.用于水合软组织生物力学的有限元方法:网格的非线性分析与自适应控制
Crit Rev Biomed Eng. 1992;20(3-4):279-313.
9
Space-time mesh adaptation for solute transport in randomly heterogeneous porous media.时空网格自适应在随机非均质地多孔介质中的溶质运移。
J Contam Hydrol. 2018 May;212:28-40. doi: 10.1016/j.jconhyd.2017.07.001. Epub 2017 Jul 5.
10
Computational modal analysis of a composite pelvic bone: convergence and validation studies.复合骨盆骨的计算模态分析:收敛性与验证研究
Comput Methods Biomech Biomed Engin. 2019 Jul;22(9):916-924. doi: 10.1080/10255842.2019.1604949. Epub 2019 Apr 19.

本文引用的文献

1
Experimental and modeling investigation of multicomponent reactive transport in porous media.多孔介质中多组分反应传输的实验与模拟研究。
J Contam Hydrol. 2011 Mar 1;120-121:27-44. doi: 10.1016/j.jconhyd.2009.11.002. Epub 2009 Dec 3.
2
A high efficiency membrane oxygenator and pulsatile pumping system, and its application to animal trials.一种高效膜式氧合器及搏动性泵血系统及其在动物试验中的应用。
Trans Am Soc Artif Intern Organs. 1973;19:72-9. doi: 10.1097/00002480-197301900-00014.